Travels In Syria And The Holy Land By John Lewis Burckhardt


























































 -  It is very
seldom crystallized; but there are sometimes nodules on the surface; it
stains the fingers of a dark - Page 322
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It Is Very Seldom Crystallized; But There Are Sometimes Nodules On The Surface; It Stains The Fingers Of A Dark Colour, And Its Fracture Is In Perpendicular Fibres.

I did not hear that the Arabs traded at all in this metal.

In Wady Osh are rocks of gneiss mixed with granite. Gneiss is found in many parts of the peninsula.

After one hour we came to a steep ascent, and descent, called El Szaleib [Arabic], which occupied two hours. We then continued our descent into the great valley called Wady el Sheikh [Arabic], one of the principal valleys of the peninsula. The rocks of Szaleib consist throughout of granite, on the upper strata of which run layers of red feldspath, some of which has fallen down and covers the valley in broken fragments. The Wady el Sheikh is broad, and has a very slight acclivity; it is much frequented by Bedouins for its pasturage. Whenever rain falls in the mountains, a stream of water flows through this Wady, and from thence through Wady Feiran, into the sea. We rode in a S.E. direction along the Wady el Sheikh for two hours, and then halted in it for the

[p.488] night, after an afternoon’s march of four hours. Several Arabs of the encampment where we slept the preceding night had joined our party, to go to the convent, for no other reason, I believe, than to get a good dinner and supper on the road. This evening eight persons kneeled down round a dish of rice, cooked with milk which I had brought from Wady Osh, and the coffee-pot being kept on the fire, we sat in conversation till near midnight.

May 1st.—We continued in a S.E. direction, ascending slightly: the valley then becomes narrower. At two hours we came to a thick wood of tamarisk or Tarfa, and found many camels feeding upon their thorny shoots. It is from this evergreen tamarisk, which grows abundantly in no other part of the peninsula, that the manna is collected. We now approached the central summits of Mount Sinai, which we had had in view for several days. Abrupt cliffs of granite from six to eight hundred feet in height, whose surface is blackened by the sun, surround the avenues leading to the elevated platform, to which the name of Sinai is specifically applied. These cliffs enclose the holy mountain on three sides, leaving the E. and N.E. sides only, towards the gulf of Akaba, more open to the view. On both sides of the wood of Tarfa trees extends a range of low hills of a substance called by the Arabs Tafal [Arabic], which I believe to be principally a detritus of the feldspar of granite, but which, at first sight, has all the appearance of pipe-clay; it is brittle, crumbles easily between the fingers, and leaves upon them its colour, which is a pale yellow. The Arabs sell it at Cairo, where it is in request for taking stains out of cloth, and where it serves the poor instead of soap, for washing their hands; but it is chiefly used to rub the skins of asses during summer, being supposed to refresh them, and to defend them against the heat of the sun.

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